2 Uncertain climate dynamics¶
2.1 approximation to climate dynamics¶
We use exponentially weighted average of each of response functions as coefficients \(\{\theta_\ell\}_{\ell=1}^L\) in our computations. The discount rate \(\delta=0.01\) and the number of climate models \(L = 144\).
The histogram of those coefficients are represented below:
import plotly.offline as pyo
from IPython.core.display import display, HTML #Added for Jupyter Books Purposes
pyo.init_notebook_mode()
from src.plots import plot2
#The Following Code is modified for Jupyter Books Purposes
pyo.plot(plot2(), filename = 'plot2.html' )
display(HTML('plot2.html'))